The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption
- Autores
- Buffan, Lucas Llilian Armand; Condamine, Fabien; Stutz, Narla Shannay; Pujos, François Roger Francis; Antoine, Pierre Olivier; Marivaux, Laurent
- Año de publicación
- 2025
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Around 34 Mya, the Eocene−Oligocene transition (EOT) marked the most dramatic global climatic cooling of the Cenozoic. On a planetary scale, paleontological evidence suggests that this transition was associated with major faunal turnovers, sometimes even regarded as a mass extinction crisis. In South America, there is no consensus on the response of the endemic mammals to this transition. Here, using a vetted fossil dataset and cutting-edge Bayesian methods, we analyzed the dynamics of South American mammal (SAM) diversification and their possible drivers across latitude (tropical vs. extratropical), taxonomic groups, and trophic guilds throughout the Eocene−Oligocene (ca. 56 to 23 Ma). Our results did not evidence any mass extinction among SAM at the EOT. Instead, they experienced a gradual and long-term diversity decline from the middle Eocene to the early Oligocene, followed by a sudden waxing-and-waning diversity associated with a large taxonomic—but not ecological—turnover. Tropical and extratropical lineages have had very distinct macroevolutionary histories. No effective change in the pace at which tropical lineages diversify was found, thus favoring the tropical stability hypothesis proposed by Wallace. Diversity-dependent effects, temperature, and Andean uplift were recovered as probable drivers of SAM diversification across the period. Contrasting evidence casts doubt on the common hypothesis primarily linking Oligocene faunal changes to grassland expansion. Our findings illustrate the uniqueness of the deep-time interplay between endemic SAM and their physical environment in a context of climatic shift, highlighting the need to consider regional idiosyncrasies for understanding the coevolution of life and climate.
Fil: Buffan, Lucas Llilian Armand. Université de Montpellier; Francia
Fil: Condamine, Fabien. Université de Montpellier; Francia
Fil: Stutz, Narla Shannay. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Université de Montpellier; Francia
Fil: Pujos, François Roger Francis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Antoine, Pierre Olivier. Université de Montpellier; Francia
Fil: Marivaux, Laurent. Université de Montpellier; Francia - Materia
-
Biological crisis
Eocene−Oligocene transition
Diversification dynamics
Multivariate analyses - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/290952
Ver los metadatos del registro completo
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The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruptionBuffan, Lucas Llilian ArmandCondamine, FabienStutz, Narla ShannayPujos, François Roger FrancisAntoine, Pierre OlivierMarivaux, LaurentBiological crisisEocene−Oligocene transitionDiversification dynamicsMultivariate analyseshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Around 34 Mya, the Eocene−Oligocene transition (EOT) marked the most dramatic global climatic cooling of the Cenozoic. On a planetary scale, paleontological evidence suggests that this transition was associated with major faunal turnovers, sometimes even regarded as a mass extinction crisis. In South America, there is no consensus on the response of the endemic mammals to this transition. Here, using a vetted fossil dataset and cutting-edge Bayesian methods, we analyzed the dynamics of South American mammal (SAM) diversification and their possible drivers across latitude (tropical vs. extratropical), taxonomic groups, and trophic guilds throughout the Eocene−Oligocene (ca. 56 to 23 Ma). Our results did not evidence any mass extinction among SAM at the EOT. Instead, they experienced a gradual and long-term diversity decline from the middle Eocene to the early Oligocene, followed by a sudden waxing-and-waning diversity associated with a large taxonomic—but not ecological—turnover. Tropical and extratropical lineages have had very distinct macroevolutionary histories. No effective change in the pace at which tropical lineages diversify was found, thus favoring the tropical stability hypothesis proposed by Wallace. Diversity-dependent effects, temperature, and Andean uplift were recovered as probable drivers of SAM diversification across the period. Contrasting evidence casts doubt on the common hypothesis primarily linking Oligocene faunal changes to grassland expansion. Our findings illustrate the uniqueness of the deep-time interplay between endemic SAM and their physical environment in a context of climatic shift, highlighting the need to consider regional idiosyncrasies for understanding the coevolution of life and climate.Fil: Buffan, Lucas Llilian Armand. Université de Montpellier; FranciaFil: Condamine, Fabien. Université de Montpellier; FranciaFil: Stutz, Narla Shannay. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Université de Montpellier; FranciaFil: Pujos, François Roger Francis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Antoine, Pierre Olivier. Université de Montpellier; FranciaFil: Marivaux, Laurent. Université de Montpellier; FranciaNational Academy of Sciences2025-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/290952Buffan, Lucas Llilian Armand; Condamine, Fabien; Stutz, Narla Shannay; Pujos, François Roger Francis; Antoine, Pierre Olivier; et al.; The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption; National Academy of Sciences; Proceedings of the National Academy of Sciences of The United States of America; 122; 20; 5-2025; 1-111091-64900027-8424CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/info:eu-repo/semantics/altIdentifier/doi/10.1073/pnas.2419520122info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-08-25T14:53:54Zoai:ri.conicet.gov.ar:11336/290952instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982026-08-25 14:53:55.304CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption |
| title |
The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption |
| spellingShingle |
The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption Buffan, Lucas Llilian Armand Biological crisis Eocene−Oligocene transition Diversification dynamics Multivariate analyses |
| title_short |
The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption |
| title_full |
The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption |
| title_fullStr |
The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption |
| title_full_unstemmed |
The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption |
| title_sort |
The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption |
| dc.creator.none.fl_str_mv |
Buffan, Lucas Llilian Armand Condamine, Fabien Stutz, Narla Shannay Pujos, François Roger Francis Antoine, Pierre Olivier Marivaux, Laurent |
| author |
Buffan, Lucas Llilian Armand |
| author_facet |
Buffan, Lucas Llilian Armand Condamine, Fabien Stutz, Narla Shannay Pujos, François Roger Francis Antoine, Pierre Olivier Marivaux, Laurent |
| author_role |
author |
| author2 |
Condamine, Fabien Stutz, Narla Shannay Pujos, François Roger Francis Antoine, Pierre Olivier Marivaux, Laurent |
| author2_role |
author author author author author |
| dc.subject.none.fl_str_mv |
Biological crisis Eocene−Oligocene transition Diversification dynamics Multivariate analyses |
| topic |
Biological crisis Eocene−Oligocene transition Diversification dynamics Multivariate analyses |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
Around 34 Mya, the Eocene−Oligocene transition (EOT) marked the most dramatic global climatic cooling of the Cenozoic. On a planetary scale, paleontological evidence suggests that this transition was associated with major faunal turnovers, sometimes even regarded as a mass extinction crisis. In South America, there is no consensus on the response of the endemic mammals to this transition. Here, using a vetted fossil dataset and cutting-edge Bayesian methods, we analyzed the dynamics of South American mammal (SAM) diversification and their possible drivers across latitude (tropical vs. extratropical), taxonomic groups, and trophic guilds throughout the Eocene−Oligocene (ca. 56 to 23 Ma). Our results did not evidence any mass extinction among SAM at the EOT. Instead, they experienced a gradual and long-term diversity decline from the middle Eocene to the early Oligocene, followed by a sudden waxing-and-waning diversity associated with a large taxonomic—but not ecological—turnover. Tropical and extratropical lineages have had very distinct macroevolutionary histories. No effective change in the pace at which tropical lineages diversify was found, thus favoring the tropical stability hypothesis proposed by Wallace. Diversity-dependent effects, temperature, and Andean uplift were recovered as probable drivers of SAM diversification across the period. Contrasting evidence casts doubt on the common hypothesis primarily linking Oligocene faunal changes to grassland expansion. Our findings illustrate the uniqueness of the deep-time interplay between endemic SAM and their physical environment in a context of climatic shift, highlighting the need to consider regional idiosyncrasies for understanding the coevolution of life and climate. Fil: Buffan, Lucas Llilian Armand. Université de Montpellier; Francia Fil: Condamine, Fabien. Université de Montpellier; Francia Fil: Stutz, Narla Shannay. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Université de Montpellier; Francia Fil: Pujos, François Roger Francis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: Antoine, Pierre Olivier. Université de Montpellier; Francia Fil: Marivaux, Laurent. Université de Montpellier; Francia |
| description |
Around 34 Mya, the Eocene−Oligocene transition (EOT) marked the most dramatic global climatic cooling of the Cenozoic. On a planetary scale, paleontological evidence suggests that this transition was associated with major faunal turnovers, sometimes even regarded as a mass extinction crisis. In South America, there is no consensus on the response of the endemic mammals to this transition. Here, using a vetted fossil dataset and cutting-edge Bayesian methods, we analyzed the dynamics of South American mammal (SAM) diversification and their possible drivers across latitude (tropical vs. extratropical), taxonomic groups, and trophic guilds throughout the Eocene−Oligocene (ca. 56 to 23 Ma). Our results did not evidence any mass extinction among SAM at the EOT. Instead, they experienced a gradual and long-term diversity decline from the middle Eocene to the early Oligocene, followed by a sudden waxing-and-waning diversity associated with a large taxonomic—but not ecological—turnover. Tropical and extratropical lineages have had very distinct macroevolutionary histories. No effective change in the pace at which tropical lineages diversify was found, thus favoring the tropical stability hypothesis proposed by Wallace. Diversity-dependent effects, temperature, and Andean uplift were recovered as probable drivers of SAM diversification across the period. Contrasting evidence casts doubt on the common hypothesis primarily linking Oligocene faunal changes to grassland expansion. Our findings illustrate the uniqueness of the deep-time interplay between endemic SAM and their physical environment in a context of climatic shift, highlighting the need to consider regional idiosyncrasies for understanding the coevolution of life and climate. |
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2025 |
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Buffan, Lucas Llilian Armand; Condamine, Fabien; Stutz, Narla Shannay; Pujos, François Roger Francis; Antoine, Pierre Olivier; et al.; The fate of South America’s endemic mammalian fauna in response to the most dramatic Cenozoic climate disruption; National Academy of Sciences; Proceedings of the National Academy of Sciences of The United States of America; 122; 20; 5-2025; 1-11 1091-6490 0027-8424 CONICET Digital CONICET |
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